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Fine root production in a chronosequence of mature reforested mangroves

The New phytologist, 2021-11, Vol.232 (4), p.1591-1602

2021

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A cautionary tale about using the apparent carbon accumulation rate (aCAR) obtained from peat cores

Scientific reports, 2021-05, Vol.11 (1), p.9547-9547, Article 9547

2021

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The effects of ditch dams on water‐level dynamics in tropical peatlands

Hydrological processes, 2021-05, Vol.35 (5), p.n/a

2021

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High permeability explains the vulnerability of the carbon store in drained tropical peatlands

Geophysical research letters, 2017-02, Vol.44 (3), p.1333-1339

2017

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Simulating the long‐term impacts of drainage and restoration on the ecohydrology of peatlands

Water resources research, 2017-08, Vol.53 (8), p.6510-6522

2017

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Bridging the gap between models and measurements of peat hydraulic conductivity

Water resources research, 2015-07, Vol.51 (7), p.5353-5364

2015

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First estimates of fine root production in tropical peat swamp and terra firme forests of the central Congo Basin

Scientific reports, 2023-07, Vol.13 (1), p.12315-12315, Article 12315

2023

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Ebullition of methane from peatlands: Does peat act as a signal shredder?

Geophysical research letters, 2015-05, Vol.42 (9), p.3371-3379

2015

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Divergent responses of permafrost peatlands to recent climate change

Environmental research letters, 2021-03, Vol.16 (3), p.34001

2021

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EnRoot: a narrow-diameter, inexpensive and partially 3D-printable minirhizotron for imaging fine root production

Plant methods, 2019-08, Vol.15 (1), p.101-101, Article 101

2019

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First Evidence of Peat Domes in the Congo Basin using LiDAR from a Fixed-Wing Drone

Remote sensing (Basel, Switzerland), 2020-07, Vol.12 (14), p.2196

2020

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high hydraulic conductivity of three wooded tropical peat swamps in northeast Peru: measurements and implications for hydrological function

Hydrological processes, 2014-04, Vol.28 (9), p.3373-3387

2014

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Water-table responses to storms in forested, drained and ditch-blocked tropical peatlands, Sebangau, Kalimantan, Indonesia

Mires and peat, 2023-01, Vol.29 (3), p.1-20

2023

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Evaluating the use of dominant microbial consumers (testate amoebae) as indicators of blanket peatland restoration

Ecological indicators, 2016-10, Vol.69, p.318-330

2016

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The forgotten forests: Incorporating temperate peat‐forming wet woodlands as nature‐based solutions into policy and practice

Ecological solutions and evidence, 2024-04, Vol.5 (2), p.n/a

2024

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The water table: Its conceptual basis, its measurement and its usefulness as a hydrological variable

Hydrological processes, 2022-06, Vol.36 (6), p.n/a

2022

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Modelling the performance of bunds and ditch dams in the hydrological restoration of tropical peatlands

Hydrological processes, 2022-01, Vol.36 (1), p.n/a

2022

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Sensitivity of mangrove soil organic matter decay to warming and sea level change

Global change biology, 2020-03, Vol.26 (3), p.1899-1907

2020

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The effect of wetting history, botanical composition and depth on the specific yield of two common types of bog peat

Hydrological processes, 2024-07, Vol.38 (7), p.n/a

2024

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Misinterpreting carbon accumulation rates in records from near-surface peat

Scientific reports, 2019-11, Vol.9 (1), p.17939-8, Article 17939

2019

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Untangling climate signals from autogenic changes in long-term peatland development

Geophysical research letters, 2015-12, Vol.42 (24), p.10,788-10,797

2015

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Ecohydrological feedbacks confound peat-based climate reconstructions

Geophysical research letters, 2012-06, Vol.39 (11), p.n/a

2012

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Controls on Saturated Hydraulic Conductivity in a Degrading Permafrost Peatland Complex

Water resources research, 2023-10, Vol.59 (10), p.n/a

2023

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Peatland pools are tightly coupled to the contemporary carbon cycle

Global change biology, 2024-01, Vol.30 (1), p.e16999-n/a

2024

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Hydroclimatic vulnerability of peat carbon in the central Congo Basin

Nature (London), 2022-12, Vol.612 (7939), p.277-282

2022

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Fine root production in a chronosequence of mature reforested mangroves

A cautionary tale about using the apparent carbon accumulation rate (aCAR) obtained from peat cores

The effects of ditch dams on water‐level dynamics in tropical peatlands

High permeability explains the vulnerability of the carbon store in drained tropical peatlands

Simulating the long‐term impacts of drainage and restoration on the ecohydrology of peatlands

Bridging the gap between models and measurements of peat hydraulic conductivity

First estimates of fine root production in tropical peat swamp and terra firme forests of the central Congo Basin

Ebullition of methane from peatlands: Does peat act as a signal shredder?

Divergent responses of permafrost peatlands to recent climate change

EnRoot: a narrow-diameter, inexpensive and partially 3D-printable minirhizotron for imaging fine root production

First Evidence of Peat Domes in the Congo Basin using LiDAR from a Fixed-Wing Drone

high hydraulic conductivity of three wooded tropical peat swamps in northeast Peru: measurements and implications for hydrological function

Water-table responses to storms in forested, drained and ditch-blocked tropical peatlands, Sebangau, Kalimantan, Indonesia

Evaluating the use of dominant microbial consumers (testate amoebae) as indicators of blanket peatland restoration

The forgotten forests: Incorporating temperate peat‐forming wet woodlands as nature‐based solutions into policy and practice

The water table: Its conceptual basis, its measurement and its usefulness as a hydrological variable

Modelling the performance of bunds and ditch dams in the hydrological restoration of tropical peatlands

Sensitivity of mangrove soil organic matter decay to warming and sea level change

The effect of wetting history, botanical composition and depth on the specific yield of two common types of bog peat

Misinterpreting carbon accumulation rates in records from near-surface peat

Untangling climate signals from autogenic changes in long-term peatland development

Ecohydrological feedbacks confound peat-based climate reconstructions

Controls on Saturated Hydraulic Conductivity in a Degrading Permafrost Peatland Complex

Peatland pools are tightly coupled to the contemporary carbon cycle

Hydroclimatic vulnerability of peat carbon in the central Congo Basin

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